| Cinder Cone | |
|---|---|
 | |
| Highest point | |
| Elevation | 1,910 m (6,270 ft) |
| Prominence | 120 m (390 ft) |
| Coordinates | 49°58′18″N123°00′25″W / 49.97167°N 123.00694°W /49.97167; -123.00694 |
| Geography | |
  Cinder Cone Location in British Columbia | |
 | |
| Location inGaribaldi Provincial Park | |
| Location | British Columbia, Canada |
| District | New Westminster Land District |
| Parent range | Garibaldi Ranges |
| Topo map | NTS 92G14Cheakamus River |
| Geology | |
| Rock age | Holocene |
| Mountain type | Cinder cone |
| Volcanic arc | Cascade Volcanic Arc |
| Volcanic belt | Garibaldi Volcanic Belt |
| Volcanic field | Garibaldi Lake volcanic field |
| Last eruption | Holocene |
Cinder Cone is acinder cone with a smallcrater on the west side of theHelm Glacier inGaribaldi Provincial Park in British Columbia, Canada. Cinder Cone is surrounded by cinder flats and its crater is filled withmeltwater during the summer. Cinder Cone is eroded easily by meltwater during the spring, washing thepyroclastics into theValley of Desolation. Cinder Cone produced a 9 km (6 mi) longlava flow during the earlyHolocene.
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